Cayuse People
The Cayuse are a Native American tribe in what is now the state of Oregon in the United States. The Cayuse tribe shares a reservation and government in northeastern Oregon with the Umatilla and the Walla Walla tribes as part of the Confederated Tribes of the Umatilla Indian Reservation. The reservation is located near Pendleton, Oregon, at the base of the Blue Mountains. The Cayuse called themselves the ''Liksiyu'' in the Cayuse language. Originally located in present-day northeastern Oregon and southeastern Washington, they lived adjacent to territory occupied by the Nez Perce and had close associations with them. Like the Plains tribes, the Cayuse placed a high premium on warfare and were skilled horsemen. They developed the Cayuse pony. The Cayuse ceded most of their traditional territory to the United States in 1855 by treaty and moved to the Umatilla Reservation, where they have formed a confederated tribe. History According to Haruo Aoki (1998), the Cayuse called ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Cayuse Lang
Cayuse may refer to: *Cayuse people, a people native to Oregon, United States *Cayuse language, an extinct language of the Cayuse people *Cayuse, Oregon, an unincorporated community in the United States *Cayuse horse, an archaic term for a feral or low-quality horse or pony * OH-6 "Cayuse", a military observation helicopter *Cayuse Five The Cayuse Five were five members of the Native American tribe, the Cayuse of Oregon who were hanged for murder, in 1850. Their names were Clokomas, Isiaasheluckas, Kiamasumkin, Telakite, and Tomahas—note how these names are spelled varies ..., five Cayuse who were hanged for murder See also *''Cayoosh Flat'' is also the old name for the town of Lillooet, British Columbia {{disambiguation ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Nez Perce People
The Nez Percé (; autonym in Nez Perce language: , meaning "we, the people") are an Indigenous people of the Plateau who are presumed to have lived on the Columbia River Plateau in the Pacific Northwest region for at least 11,500 years.Ames, Kenneth and Alan Marshall. 1980. "Villages, Demography and Subsistence Intensification on the Southern Columbia Plateau". ''North American Archeologist'', 2(1): 25–52." Members of the Sahaptin language group, the Nimíipuu were the dominant people of the Columbia Plateau for much of that time, especially after acquiring the horses that led them to breed the appaloosa horse in the 18th century. Prior to first contact with European colonial people the Nimiipuu were economically and culturally influential in trade and war, interacting with other indigenous nations in a vast network from the western shores of Oregon and Washington, the high plains of Montana, and the northern Great Basin in southern Idaho and northern Nevada. French explor ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Deschutes River (Oregon)
The Deschutes River in central Oregon is a major tributary of the Columbia River. The river provides much of the drainage on the eastern side of the Cascade Range in Oregon, gathering many of the tributaries that descend from the drier, eastern flank of the mountains. The Deschutes provided an important route to and from the Columbia for Native Americans for thousands of years, and then in the 19th century for pioneers on the Oregon Trail. The river flows mostly through rugged and arid country, and its valley provides a cultural heart for central Oregon. Today the river supplies water for irrigation and is popular in the summer for whitewater rafting and fishing. The river flows generally north, as do several other large Oregon tributaries of the Columbia River, including the Willamette and John Day. Course The headwaters of the Deschutes River are at Little Lava Lake, a natural lake in the Cascade Range approximately northwest of the city of La Pine. The river flows s ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
John Day River
The John Day River is a tributary of the Columbia River, approximately long, in northeastern Oregon in the United States. It is known as the Mah-Hah River by the Cayuse people, the original inhabitants of the region. Undammed along its entire length, the river is the fourth longest free-flowing river in the contiguous United States. There is extensive use of its waters for irrigation. Its course furnishes habitat for diverse species, including wild rainbow trout, steelhead and Chinook salmon runs."John Day Subbasin Plan", p. 31 However, the steelhead populations are under federal Endangered Species Act (ESA) protections, and the Chinook salmon have been proposed for such protection. The river was named for John Day (fur trader), John Day, a member of the Astor Expedition, Pacific Fur Company's overland expedition to the mouth of the Columbia River that left Missouri in 1810. Day struggled through eastern Oregon during the winter of 1811–12. While descending the Columbia River ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Powder River (Oregon)
The Powder River is a tributary of the Snake River, approximately long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed May 3, 2011 in northeast Oregon in the United States. It drains an area of the Columbia Plateau on the eastern side of the Blue Mountains. It flows almost entirely within Baker County but downstream of the city of North Powder forms part of the border between Baker County and Union County. Name The name ''Powder River'' is first recorded in the journals of Peter Skene Ogden without notation of the origin of the name. Explorer Donald Mackenzie likely named the river. William C. McKay, grandson of John Jacob Astor's partner Alexander MacKay, says that the origin of the name is from the powdery and sandy soil along the shores of the river, from the Chinook Jargon ''polalle illahe''. It appears on Lewis and Clark's maps as ''Port-pel-lah''. Course The Powder River's tributaries arise in the southern ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Burnt River (Oregon)
The Burnt River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed May 3, 2011 tributary of the Snake River in eastern Oregon, United States. It enters the Snake near Huntington, Oregon, at a point upstream of the Powder River and downstream of the Malheur River, slightly more than from the Snake's confluence with the Columbia River. Draining , it flows predominantly west to east. The river begins at Unity Reservoir at the confluence of the North, West, Middle, and South forks of the river. The reservoir is slightly east of the Wallowa-Whitman National Forest in the Blue Mountains and slightly north of Unity. Unity Lake State Recreation Site adjoins the reservoir. As it leaves the lake, the river flows under Oregon Route 245, then runs east through the upper Burnt River Valley past Hereford and Bridgeport and, through the Burnt River Canyon, to Durkee. Turning generally south at Durkee, the river runs along Inte ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Grande Ronde River
The Grande Ronde River ( or, less commonly, ) is a tributary of the Snake River, long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed May 3, 2011 in northeastern Oregon and southeastern Washington in the United States. It drains an area southeast of the Blue Mountains and northwest of the Wallowa Mountains, on the Columbia Plateau. It flows through the agricultural Grande Ronde Valley in its middle course and through a series of scenic canyons in its lower course. Course The Grande Ronde River rises in the Blue Mountains near the Anthony Lakes recreation area in the Wallowa–Whitman National Forest in southwestern Union County approximately south of La Grande. It flows generally north along the east side of the Blue Mountains, then east, past La Grande, then generally northeast through the Grande Ronde Valley in a meandering course between the Blue Mountains and the Wallowa Mountains, receiving Catherine Creek east ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Umatilla River
The Umatilla River is an tributary of the Columbia River in northern Umatilla County, Oregon, United States. Draining a basin of , it enters the Columbia near the city of Umatilla in the northeastern part of the state. In downstream order, beginning at the headwaters, major tributaries of the Umatilla River are the North Fork Umatilla River and the South Fork Umatilla River, then Meacham, McKay, Birch, and Butter creeks. The name ''Umatilla'' is derived from the Native American autonym of the people residing along its banks - the Umatilla, which called themselves Imatalamłáma - "People from the Village Ímatalam n the Peninsula formed by the confluence of Umatilla River with the Columbia, which was first recorded as ''Youmalolam'' in the journals of the Lewis and Clark Expedition and spelled in many other ways in early books about Oregon.McArthur, p. 981 Today the river is also called Nixyáawi wána - "Pendleton area River, i.e. Umatilla River". Course The Umatilla Ri ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Touchet River
The Touchet River is a tributary of the Walla Walla River in southeastern Washington in the United States. The Touchet River drains an area of about in Columbia County and Walla Walla County.Washington Road & Recreation Atlas, Benchmark Maps, Medford, Oregon, 2002 The upper Touchet was a traditional summer meeting place for trade and games for the Palus, Nez Perce and Walla Walla tribes. The name Touchet derives from the similarly pronounced Sahaptin term for the river, ''Tu-se'' meaning roasting. Nez Perce legend tells that coyote roasted salmon at this river after breaking a fish dam guarded by the seven swallow sisters at Celilo. The USGS cited two variant names, Pouchet River and Toosha River. Geography The Touchet River is formed by several forks draining the north slope of the Blue Mountains above Dayton in Columbia County. All the forks have their head in the Walla Walla Ranger District of the Umatilla National Forest. The North Fork, about long, begins near Ski Bl ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Walla Walla River
The Walla Walla River is a tributary of the Columbia River, joining the Columbia just above Wallula Gap in southeastern Washington (state), Washington in the United States. The river flows through Umatilla County, Oregon, and Walla Walla County, Washington. Its drainage basin is in area.Walla Walla Subbasin Plan Northwest Power and Conservation Council Course The headwaters of the Walla Walla River lie in the Blue Mountains (Oregon), Blue Mountains of northeastern Oregon. The river originates as the North and South Forks of the Walla Walla River. The surrounding forested land holds a network of hiking and mountain-biking trails. The confluence of the North and South Forks lies east of Milton-Freewater, Oregon, Milton–Freewater, Oregon. The river flows eastward to reach ...[...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Tucannon River
The Tucannon River is a tributary of the Snake River in the U.S. state of Washington. It flows generally northwest from headwaters in the Blue Mountains of southeastern Washington to meet the Snake upstream from Lyons Ferry Park and the mouth of the Palouse River. The Tucannon is about long. Part of the upper river flows through the Wenaha–Tucannon Wilderness. Watershed The Tucannon basin of ranges in elevation from about above sea level at the mouth on the Snake River to about in the Umatilla National Forest of the Blue Mountains. River flows in the Tucannon basin depend solely on precipitation and groundwater. Studies in the early 1990s suggested that these flows would not be able to meet all of the claims, public and private, on the water resources of the lower river. In particular, farm irrigation projects were competing with fisheries for limited water. The Washington Department of Ecology named the Tucannon basin a Watershed Resource Inventory Area (WRIA) and in 1995 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Snake River
The Snake River is a major river of the greater Pacific Northwest region in the United States. At long, it is the largest tributary of the Columbia River, in turn, the largest North American river that empties into the Pacific Ocean. The Snake River rises in western Wyoming, then flows through the Snake River Plain of southern Idaho, the rugged Hells Canyon on the Oregon–Idaho border and the rolling Palouse Hills of Washington (state), Washington, emptying into the Columbia River at the Tri-Cities, Washington, Tri-Cities in the Columbia Basin of Eastern Washington. The Snake River drainage basin encompasses parts of six U.S. states (Idaho, Washington, Oregon, Utah, Nevada, and Wyoming) and is known for its varied geologic history. The Snake River Plain was created by a volcanic hotspot (geology), hotspot which now lies underneath the Snake River headwaters in Yellowstone National Park. Gigantic glacial-retreat flooding episodes during the previous Last glacial period, Ice Ag ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |